Department of Chemistry, Stanford University, Stanford, California 94305, USA.
J Am Chem Soc. 2013 Jan 23;135(3):1124-36. doi: 10.1021/ja3103583. Epub 2013 Jan 10.
The electronic structure of the Fe-O(2) center in oxy-hemoglobin and oxy-myoglobin is a long-standing issue in the field of bioinorganic chemistry. Spectroscopic studies have been complicated by the highly delocalized nature of the porphyrin, and calculations require interpretation of multideterminant wave functions for a highly covalent metal site. Here, iron L-edge X-ray absorption spectroscopy, interpreted using a valence bond configuration interaction multiplet model, is applied to directly probe the electronic structure of the iron in the biomimetic Fe-O(2) heme complex [Fe(pfp)(1-MeIm)O(2)] (pfp ("picket fence porphyrin") = meso-tetra(α,α,α,α-o-pivalamidophenyl)porphyrin or TpivPP). This method allows separate estimates of σ-donor, π-donor, and π-acceptor interactions through ligand-to-metal charge transfer and metal-to-ligand charge transfer mixing pathways. The L-edge spectrum of [Fe(pfp)(1-MeIm)O(2)] is further compared to those of [Fe(II)(pfp)(1-MeIm)(2)], [Fe(II)(pfp)], and [Fe(III)(tpp)(ImH)(2)]Cl (tpp = meso-tetraphenylporphyrin) which have Fe(II)S = 0, Fe(II)S = 1, and Fe(III)S = 1/2 ground states, respectively. These serve as references for the three possible contributions to the ground state of oxy-pfp. The Fe-O(2) pfp site is experimentally determined to have both significant σ-donation and a strong π-interaction of the O(2) with the iron, with the latter having implications with respect to the spin polarization of the ground state.
在生物无机化学领域,血红素和肌红蛋白中 Fe-O(2)中心的电子结构一直是一个悬而未决的问题。光谱研究受到卟啉高度离域性质的影响,而计算则需要对高度共价的金属位点的多行列式波函数进行解释。在这里,我们应用铁边 X 射线吸收光谱,使用价键组态相互作用多组态模型进行解释,直接探测仿生 Fe-O(2)血红素配合物[Fe(pfp)(1-MeIm)O(2)](pfp(“尖桩篱笆卟啉”)= 间位 - 四(α,α,α,α-o-新戊酰基苯基)卟啉或 TpivPP)中铁的电子结构。这种方法允许通过配体到金属电荷转移和金属到配体电荷转移混合途径,分别估计 σ-供体、π-供体和π-受体相互作用。[Fe(pfp)(1-MeIm)O(2)]的 L 边谱进一步与 [Fe(II)(pfp)(1-MeIm)(2)]、[Fe(II)(pfp)]和 [Fe(III)(tpp)(ImH)(2)]Cl(tpp = 间位 - 四苯基卟啉)的 L 边谱进行比较,它们分别具有 Fe(II)S = 0、Fe(II)S = 1 和 Fe(III)S = 1/2 的基态。这些谱线分别为 oxy-pfp 的三种可能基态贡献提供了参考。实验确定,Fe-O(2)pfp 位点具有显著的 σ-供体和 O(2)与铁的强 π 相互作用,后者对基态的自旋极化具有重要意义。